Sulfates
are compounds of oxygen and sulphur combined with one or more metals.
The oxygen and sulphur come together to create the sulfate ion,
SO4-2, in which the central Sulphur atom is surrounded
by four oxygen atoms located at the corners of a tetrahedron. The
two negative
charges are distributed evenly over the oxygen atoms.
The sulfates
are complex minerals. This happens because of the large number
of ways in which metal ions can be placed amongst
the sulfate groups in the crystal structure. Many of the minerals
are strongly hydrated species, meaning that they are bound with
water molecules in the crystal. Most are rare, although gypsum
and anhydrite are quite common minerals.
All minerals in the group are translucent to transparent. Many
are light in colour. A few are very soluble in water, making
them relatively rare minerals. None are hard, but most are fairly
high in specific gravity becuse of the relatively dense metal
packing in the crystal structure.